Assessment of Ba/Ca in Arctica islandica shells as a proxy for phytoplankton dynamics in the Northwestern Atlantic Ocean

Despite its major role as a global climate regulator, little is known about the recent evolution of the North Atlantic Ocean, especially prior to the fifties, principally because of the lack of long-term instrumental data. Moreover, the North Atlantic Ocean is undergoing rapid changes at the physica...

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Bibliographic Details
Published in:Estuarine, Coastal and Shelf Science
Main Authors: Doré, Justine, Chaillou, Gwénaelle, Poitevin, Pierre, Lazure, Pascal, Poirier, André, Chauvaud, Laurent, Archambault, Philippe, Thébault, Julien
Format: Article in Journal/Newspaper
Language:English
Published: Elsevier BV 2020
Subjects:
A. islandica
Ba/Ca
Master chronology
Cross-dating
Chlorophyll a
Northwestern Atlantic
Arctica islandica
North Atlantic
Online Access:https://archimer.ifremer.fr/doc/00607/71881/70576.pdf
https://doi.org/10.1016/j.ecss.2020.106628
https://archimer.ifremer.fr/doc/00607/71881/
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Summary:Despite its major role as a global climate regulator, little is known about the recent evolution of the North Atlantic Ocean, especially prior to the fifties, principally because of the lack of long-term instrumental data. Moreover, the North Atlantic Ocean is undergoing rapid changes at the physical scale leading to modifications at the biological scale increasing interest to monitor the environment. The phytoplankton is the base of the ocean life and its perturbation can lead to further changes in the food chain. Recording its dynamics implies to observe both its spatial and temporal variations. This study brings forward the use of the Ba/Ca ratio from shells of the long-living bivalve Arctica islandica collected in the Northwestern Atlantic Ocean near Saint-Pierre and Miquelon (SPM) as a recorder of the past and present phytoplankton dynamics. A high inter and intra-reproducibility and synchrony between Ba/Cashell profiles were demonstrated allowing the reconstruction of a 124 years annually-resolved Ba/Cashell master chronology (from 1893 to 2016). This master chronology was positively correlated to the surface chlorophyll a measured by satellite sensor at regional (around SPM) and global scales (Northwestern Atlantic).

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